dc.contributor.author |
Sidorova E.U. |
|
dc.contributor.author |
Sitdikova L.M. |
|
dc.contributor.author |
Izotov V.G. |
|
dc.contributor.author |
Khasanova N.M. |
|
dc.date.accessioned |
2021-02-25T06:52:56Z |
|
dc.date.available |
2021-02-25T06:52:56Z |
|
dc.date.issued |
2020 |
|
dc.identifier.issn |
1755-1307 |
|
dc.identifier.uri |
https://dspace.kpfu.ru/xmlui/handle/net/161237 |
|
dc.description.abstract |
© 2020 IOP Publishing Ltd. All rights reserved. The studied weathering crust on the basement rocks of the central part of the Volga-Ural anteclise lies at great depths under thick sediments of sedimentary cover. A diversity of initial basement rocks, features of formation and secondary changing processes of weathering crust determine interest for this geological formation and its uniqueness. Clay minerals play a major role in the composition of the weathering crust and determine its features. A change in the associations of clay minerals by the weathering profile allows distinguishing different zones, which confirm the zonal structure of this formation. |
|
dc.relation.ispartofseries |
IOP Conference Series: Earth and Environmental Science |
|
dc.title |
The role of the leading formations of crystalline basement in the generation of clay minerals of weathering crust (East of the Russian plate) |
|
dc.type |
Conference Paper |
|
dc.relation.ispartofseries-issue |
1 |
|
dc.relation.ispartofseries-volume |
516 |
|
dc.collection |
Публикации сотрудников КФУ |
|
dc.source.id |
SCOPUS17551307-2020-516-1-SID85087447263 |
|